Regional and seasonal hydrological changes with and without Stratospheric Aerosol Intervention under High Greenhouse Gas climates

16 views
Skip to first unread message

Geoengineering News

unread,
May 24, 2025, 10:07:33 AM5/24/25
to geoengi...@googlegroups.com
https://essopenarchive.org/doi/full/10.22541/essoar.174708323.34069174

Authors
Abolfazl Rezaei,
John Christopher Moore,
Simone Tilmes,
Khalil Karami

12 May 2025

Abstract
Stratospheric aerosol intervention (SAI) is being explored for its potential to reduce greenhouse gas (GHG) induced climate damages. We assess the effectiveness of two SAI experiments, G6Sulfur and Geo SSP5-8.5 1.5‎ (here called Geo-SAI), using the CESM2(WACCM6) model, to reduce hydrological changes under high-emission SSP5-8.5 (no mitigation) pathway. Geo-SAI stabilizes near surface global temperatures at 1.5℃ above pre-industrial levels, while G6Sulfur limits temperature rises to those under the SSP2-4.5 scenario. In our findings, Geo-SAI reverts many, but not all, hydrological changes induced by SSP5-8.5, restoring global and regional means, seasonal amplitudes, and peak timings. G6Sulfur delivers smaller restorations, as expected, due to its smaller prescribed forcing. In hyper-arid regions such as the Middle East, both SAI scenarios improve water storage compared with both SSP5-8.5 and present conditions. However, in wetter or cooler climates, such as the Amazon, middle and southern Africa and east Europe, they only partly reverse the reductions in available water (AW) and runoff caused by high GHG emissions. Residual warming and snowmelt dynamics play an important role in runoff at mid-to-high latitudes. Additionally, SAI does not completely suppress GHG-induced vegetation expansion and so over-reduces global runoff in three latitude bands: 45-65°N, 45-65°S, and 30°S to 0, with end‐of‐century decreases of 4.1% under G6Sulfur and 7.3% under Geo-SAI, despite mean AW levels remaining close to present-day. These findings emphasize that while SAI mitigates many climate-driven hydrological disruptions, its unintended effects on runoff, vegetation feedbacks, and regional water availability warrants study—especially in regions heavily dependent on surface water resources.

Source: ESS OPEN ARCHIVES
Reply all
Reply to author
Forward
0 new messages